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    • Journal of Range Management, Volume 43 (1990)
    • Journal of Range Management, Volume 43, Number 5 (September 1990)
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    Effect of grazing and cultivation on some chemical properties of soils in the mixed prairie

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    Author
    Dormaar, J. F.
    Willms, W. D.
    Issue Date
    1990-09-01
    Keywords
    grassland soils
    soil organic matter
    tillage
    monosaccharides
    organic acids and salts
    soil quality
    transformation
    physicochemical properties
    chernozemic soils
    mixed pastures
    Hesperostipa comata
    Alberta
    pastures
    Bouteloua gracilis
    prairies
    grazing
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    Citation
    Dormaar, J. F., & Willms, W. D. (1990). Effect of grazing and cultivation on some chemical properties of soils in the mixed prairie. Journal of Range Management, 43(5), 456-460.
    Publisher
    Society for Range Management
    Journal
    Journal of Range Management
    URI
    http://hdl.handle.net/10150/644854
    DOI
    10.2307/3899012
    Additional Links
    https://rangelands.org/
    Abstract
    Components of the organic matter were studied in soil under 3 Mixed Prarie types: grassland dominated by needle-and-thread/blue grama (Stipa comata Trin. and Rupr./Bouteloua gracilis (HBK.) Lag. ex Steud.) in good range condition; grassland significantly modified by grazing, dominated by blue grama and in poor range condition; and grassland, dominated by needle-and-thread/blue grama in good range condition, but converted to cropland and under continuous wheat for 4 years. The soils were sampled on 13 April 1988. Concentrations of total organic carbon in the upper 2 cm were 1.39, 2.70, and 1.87%, respectively. The higher organic carbon under blue grama was caused by an active, ramified, fine rootmass which gave rise to most of the monosaccharides being of microbial origin. The monosaccharides in the lower Ap horizon in the cropland were generally of plant origin from incorporated straw. The Ah horizons of the needle-and-thread/blue grama and blue grama sites and the Ap horizon of the cultivated site yielded 244, 696, and 370 migrograms g-1 organic acids in the alkaline-soluble fraction of the soil, respectively. Although most of the organic compounds identified were present in all 3 soils, the quantitative patterns were quite different. Differences exist due to inputs by different species, and 4 years of cropping also made significant soil chemical changes. This study demonstrated the importance of recognizing the history of the soils studied when describing soil quality.
    Type
    text
    Article
    Language
    en
    ISSN
    0022-409X
    ae974a485f413a2113503eed53cd6c53
    10.2307/3899012
    Scopus Count
    Collections
    Journal of Range Management, Volume 43, Number 5 (September 1990)

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